The coadsorption of oxygen and chlorine is studied on the Pt(111) surf
ace, using line-of-sight desorption mass spectrometry, LEED and work f
unction measurements to characterize the resulting adlayers and to det
ermine the uptake and desorption kinetics. Preadsorbed chlorine reduce
s the sticking probability of oxygen to a similar extent, as does an e
qual concentration of adsorbed oxygen atoms. Chlorine adsorption proce
eds in the whole range of possible oxygen precoverages (less than or e
qual to 0.25) with a similar sticking coefficient as on the clean surf
ace and leads to a high density adlayer with a total concentration of
11.3 x 10(14) (O + Cl)atoms cm(-2) Starting with a complete (2 x 2) ox
ygen adlayer, the ordered structure vanishes during chlorine dosing on
ly at a total coverage (chlorine plus oxygen) of 0.5. Increasing the t
otal concentration further leads to the buildup of a (3 root 3 x 3 roo
t 3)R30 degrees structure at 9.3 x 10(14)(O+Cl) atoms cm(-2). Temperat
ure-programmed desorption yields oxygen molecules, chlorine molecules
and chlorine atoms. The two adsorbed species destabilize each other, a
nd the molecule peaks are shifted to lower temperatures, in the case o
f oxygen up to 70 K. With high initial coverages, this trend is not co
ntinued but reversed. (C) 1998 Elsevier Science B.V. All rights reserv
ed.